testfield trento: geometric evaluation of very high

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TESTFIELD TRENTO: GEOMETRIC EVALUATION OF VERY HIGH RESOLUTION SATELLITE IMAGERY G. Agugiaro a , D. Poli b , F. Remondino a a 3D Optical Metrology unit, Bruno Kessler Foundation, Trento, Italy {agugiaro, remondino}@fbk.eu, http://3dom.fbk.eu b Vermessung AVT ZT-GmbH, Austria [email protected], http://www.avt.at Commission I – WG4 KEY WORDS: Testfield, Very High Resolution, GeoEye-1, WorldView-2, Digital Surface Modelling, Quality Analysis ABSTRACT: Today the use of spaceborne Very High Spatial Resolution (VHSR) optical sensors for automatic 3D information extraction is increasing in the scientific and civil communities. The 3D Optical Metrology (3DOM) Unit of the Bruno Kessler Foundation (FBK) in Trento (Italy) has collected stereo VHSR satellite imagery, as well as aerial and terrestrial data over Trento, with the aim to create a complete data collection with state-of-the-art datasets for investigations on image analysis, automatic digital surface model (DSM) generation, 2D/3D feature extraction, city modelling and data fusion. The testfield region covers the city of Trento, characterised by very dense urban (historical centre), residential and industrial areas, and the surrounding hills and steep mountains (approximate height range 200-2100 m) with cultivations, forests and bare soil. This paper reports the analysis conducted in FBK on the VHSR spaceborne imagery of Trento testfield for 3D information extraction. The data include two stereo-pairs acquired by WorldView-2 in August 2010 and by GeoEye-1 in September 2011 in panchromatic and multispectral mode, together with their original Rational Polynomial Coefficients (RPC), and the position and description of well distributed ground points. For reference and validation, a DSM from airborne LiDAR acquisition is used. The paper gives details on the project and the dataset characteristics. The results achieved by 3DOM on DSM extraction from WorldView-2 and GeoEye-1 stereo-pairs are shown and commented. 1. INTRODUCTION The 3D Optical Metrology (3DOM) unit of the Bruno Kessler Foundation (FBK) in Trento (Italy) is building a testfield by collecting high resolution (HR) and very high resolution (VHR) satellite imagery, airborne and UAV images and orthophotos, LiDAR scans, and a network of circa 70 ground control points. The testfield region is centred on the city of Trento, characterised by an historical centre, residential and industrial areas and is surrounded by hills and steep mountains, with a variety of differently agricultural areas, forests and bare soil. The aim is to build state-of-the-art datasets to test methods and algorithms for image radiometric analysis, triangulation and geo-referencing, automatic surface modelling, 2D/3D feature extraction, change detection and data fusion. This paper focuses on the processing of the very high resolution (VHR) satellite imagery available in the testfield for digital surface model (DSM) extraction. Spaceborne VHR optical sensors are able to scan any point of the Earth surface with a ground spatial resolution around half meter and a revisit time in the order of few days; through their very agile manoeuvring they can also acquire stereo data within the same orbit just using the CCD line combination, by pointing at the same area from two or more orbit positions (Poli and Toutin, 2012). Thanks to the improved acquisition technology, this new class of VHR sensors allows surface modelling up to building level of detail, in 2.5D (DSM) or even in 3D (object extraction) (Poli et al. 2009; Arefi and Reinartz, 2011; d’Angelo and Reinartz, 2011; Capalbo et al., 2012; Poli and Caravaggi, 2012). The paper introduces the project, with information on the testfield characteristics and activity plan, and describes the processing carried out on WorldView-2 and GeoEye-1 stereo- pairs. The images were oriented using the available ground control points and digital surface models were generated with area- and feature-based least-square image matching. The DSMs were compared both qualitatively (visual analysis) and quantitatively, using the LIDAR as reference. The results are presented and commented. 2. TEST AREA AND DATA SOURCES The test area is located in Trento, a city of about 115.000 inhabitants in the Trentino-Alto Adige region (Northeast of Italy). It lies on the banks of the river Adige in the homonymous valley (North-South direction) and is surrounded East and West, by the Alps (Fig. 1). The testfield varies from urban areas with residential, industrial and commercial buildings at different sizes and heights, to agricultural or forested areas, and rocky steep surfaces, offering therefore a heterogeneous landscape in term of geometrical complexity, land use and cover. The city of Trento lies circa 200 m a.s.l., while the nearby peaks reach as high as 2100 m. 2.1 Data sources Several heterogeneous datasets were identified or collected at varying spatial resolution, ranging from satellite imagery to aerial imagery, LiDAR data, GNSS surveyed points, GIS data, etc. A global overview about the extents of the areas covered by each type of imagery data is given in Fig. 1. For completeness, existing data available also from other institutions on the territory (e.g. the Autonomous Province of Trento, the Municipality of Trento, RSLab of the University of Trento) are mentioned in the following list. The spaceborne data are summarised in Table 1 and include: - WorldView-2 (WV2) stereo-pair: the processing level is Stereo 1B, i.e. the images are radiometrically and sensor corrected, but not projected to a plane using a map projection or datum, thus keeping the original acquisition geometry. The available channels are the panchromatic one and eight multispectral ones. In addition to the standard multispectral bands (blue, green, red, near infrared), International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B1, 2012 XXII ISPRS Congress, 25 August – 01 September 2012, Melbourne, Australia 191

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Page 1: TESTFIELD TRENTO: GEOMETRIC EVALUATION OF VERY HIGH

TESTFIELD TRENTO:

GEOMETRIC EVALUATION OF VERY HIGH RESOLUTION SATELLITE IMAGERY

G. Agugiaro a, D. Poli

b, F. Remondino

a

a 3D Optical Metrology unit, Bruno Kessler Foundation, Trento, Italy

{agugiaro, remondino}@fbk.eu, http://3dom.fbk.eu b Vermessung AVT ZT-GmbH, Austria

[email protected], http://www.avt.at

Commission I – WG4

KEY WORDS: Testfield, Very High Resolution, GeoEye-1, WorldView-2, Digital Surface Modelling, Quality Analysis

ABSTRACT: Today the use of spaceborne Very High Spatial Resolution (VHSR) optical sensors for automatic 3D information extraction is increasing in the scientific and civil communities. The 3D Optical Metrology (3DOM) Unit of the Bruno Kessler Foundation (FBK)

in Trento (Italy) has collected stereo VHSR satellite imagery, as well as aerial and terrestrial data over Trento, with the aim to create a complete data collection with state-of-the-art datasets for investigations on image analysis, automatic digital surface model (DSM)

generation, 2D/3D feature extraction, city modelling and data fusion. The testfield region covers the city of Trento, characterised by

very dense urban (historical centre), residential and industrial areas, and the surrounding hills and steep mountains (approximate height range 200-2100 m) with cultivations, forests and bare soil.

This paper reports the analysis conducted in FBK on the VHSR spaceborne imagery of Trento testfield for 3D information extraction. The data include two stereo-pairs acquired by WorldView-2 in August 2010 and by GeoEye-1 in September 2011 in panchromatic and multispectral mode, together with their original Rational Polynomial Coefficients (RPC), and the position and

description of well distributed ground points. For reference and validation, a DSM from airborne LiDAR acquisition is used. The paper gives details on the project and the dataset characteristics. The results achieved by 3DOM on DSM extraction from

WorldView-2 and GeoEye-1 stereo-pairs are shown and commented.

1. INTRODUCTION

The 3D Optical Metrology (3DOM) unit of the Bruno Kessler

Foundation (FBK) in Trento (Italy) is building a testfield by

collecting high resolution (HR) and very high resolution (VHR) satellite imagery, airborne and UAV images and orthophotos, LiDAR scans, and a network of circa 70 ground control points.

The testfield region is centred on the city of Trento, characterised by an historical centre, residential and industrial

areas and is surrounded by hills and steep mountains, with a variety of differently agricultural areas, forests and bare soil. The aim is to build state-of-the-art datasets to test methods and

algorithms for image radiometric analysis, triangulation and geo-referencing, automatic surface modelling, 2D/3D feature

extraction, change detection and data fusion. This paper focuses on the processing of the very high resolution (VHR) satellite imagery available in the testfield for digital

surface model (DSM) extraction. Spaceborne VHR optical sensors are able to scan any point of the Earth surface with a

ground spatial resolution around half meter and a revisit time in

the order of few days; through their very agile manoeuvring

they can also acquire stereo data within the same orbit just using the CCD line combination, by pointing at the same area from two or more orbit positions (Poli and Toutin, 2012). Thanks to

the improved acquisition technology, this new class of VHR sensors allows surface modelling up to building level of detail,

in 2.5D (DSM) or even in 3D (object extraction) (Poli et al. 2009; Arefi and Reinartz, 2011; d’Angelo and Reinartz, 2011;

Capalbo et al., 2012; Poli and Caravaggi, 2012).

The paper introduces the project, with information on the testfield characteristics and activity plan, and describes the

processing carried out on WorldView-2 and GeoEye-1 stereo-pairs. The images were oriented using the available ground

control points and digital surface models were generated with area- and feature-based least-square image matching. The DSMs were compared both qualitatively (visual analysis) and

quantitatively, using the LIDAR as reference. The results are presented and commented.

2. TEST AREA AND DATA SOURCES

The test area is located in Trento, a city of about 115.000 inhabitants in the Trentino-Alto Adige region (Northeast of

Italy). It lies on the banks of the river Adige in the homonymous valley (North-South direction) and is surrounded East and West,

by the Alps (Fig. 1). The testfield varies from urban areas with residential, industrial and commercial buildings at different sizes and heights, to agricultural or forested areas, and rocky

steep surfaces, offering therefore a heterogeneous landscape in term of geometrical complexity, land use and cover. The city of

Trento lies circa 200 m a.s.l., while the nearby peaks reach as high as 2100 m.

2.1 Data sources

Several heterogeneous datasets were identified or collected at varying spatial resolution, ranging from satellite imagery to

aerial imagery, LiDAR data, GNSS surveyed points, GIS data, etc. A global overview about the extents of the areas covered by

each type of imagery data is given in Fig. 1. For completeness, existing data available also from other institutions on the

territory (e.g. the Autonomous Province of Trento, the Municipality of Trento, RSLab of the University of Trento) are mentioned in the following list.

The spaceborne data are summarised in Table 1 and include:

- WorldView-2 (WV2) stereo-pair: the processing level is Stereo 1B, i.e. the images are radiometrically and sensor

corrected, but not projected to a plane using a map projection or datum, thus keeping the original acquisition

geometry. The available channels are the panchromatic one

and eight multispectral ones. In addition to the standard multispectral bands (blue, green, red, near infrared),

International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B1, 2012 XXII ISPRS Congress, 25 August – 01 September 2012, Melbourne, Australia

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Page 2: TESTFIELD TRENTO: GEOMETRIC EVALUATION OF VERY HIGH

Figure 1. [Left] Approximate spatial extents of satellite and aerial imagery over the Trento testfield. The extents of each imagery type

projected onto the DSM: WorldView-2 stereo-pair (red), GeoEye-1 stereo-pair (yellow), Quickbird scenes (green and cyan), aerial (white) and UAV (violet). SPOT imagery is not depicted, as it comprises the whole area. [Right] Distribution of ground points with

respect to WorldView-2 (red) and GeoEye-1 (yellow) imagery extent, with corresponding metadata and photographic information.

WorldView-2 scans in the coastal (400-450 nm), yellow (585-625 nm), red edge (705-745 nm) and near infrared-2

(860-1040 nm) spectral ranges. The images cover an area of 17.64×17.64 km and have an overlap of 100%. The images were provided with Rational Polynomial Coefficients

(RPCs).

- GeoEye-1 (GE1) stereo-pair: the stereo images have 100%

overlap and are provided as GeoStereo product, that is, they are projected to a constant base elevation. The available bands are the panchromatic one and four multispectral

bands (blue, green, red, and near infrared). The images cover an area of 10×10 km. For each image the RPCs were

provided. - Quickbird images: two single scenes were acquired on 30

October 2005 and 17 July 2006, respectively. The

panchromatic and multispectral channels are available. - SPOT-5 images: a scene was acquired over Trento on 31

August 2008 with the HRG sensor (2.5 m GSD, panchromatic) and VEGETATION sensor (10 m GSD,

multispectral).

The airborne data include:

- A raster-based DSM (with the filtered DTM) derived from a LiDAR flight in 2006/7 at ca. 1.3 points/m2. The DSM has a

grid space of 1 m (2 m in some scarcely inhabited mountainous areas). The height accuracy for the original

LiDAR data is given as σz=15 cm for the DSM, and σz=30

cm for the DTM. The LiDAR DSM was considered the reference dataset for the geometric analyses.

- A set of 230 digital orthophotos produced in 2006 and 2009,

with a ground sample distance (GSD) of 50 cm. - A block of 10 nadir aerial images acquired in 2009 with a

RMKTOP15 analogic camera over the city of Trento (overlap of 60% along track and 30% across track). The digitised images have an average GSD of ca. 12 cm.

- A block of about 180 UAV images acquired in January 2012 with a Microdrones MD4-200 mounting a Pentax

Optio A40 digital camera (overlap of 80% along track and

40% across track). The images have an average GSD of ca.

3 cm.

Other data include:

- About 70 ground points, acquired in spring/summer 2011 by

means of a GNSS receiver and post-processed using the

Trento GNSS permanent station in order to achieve sub-decimetre accuracy.

- 12 ground points, located on building corners and roofs

acquired in January 2012 by Total Station.

- GIS vector data for the whole province of Trento, consisting (mainly) of a topographic map at nominal scale of 1:10000,

and a set of 447 cadastral maps in vector format at nominal scale of 1:1000.

Table 1. Characteristics of satellite imagery in the Trento testfield. PAN: panchromatic, MS4: multispectral (4 bands), MS8: multispectral (8 bands), GSD: Ground Sample Distance.

Sensor Acquisition

date Bands

Avg.

GSD

[m]

Size x

[km]

Size y

[km] Licensee

Quickbird 30 Oct 2005 PAN

MS4

0.6

2.4 14,75 7,51 Univ. Trento

Quickbird 17 Jul 2006 PAN MS4

0.6 2.4

15,08 9,20 Univ. Trento

SPOT5-VEG 31 Aug 2006 MS4 10.0 36,28 36,13 Univ. Trento

SPOT5-HRG 31 Aug 2006 PAN 2.5 36,22 36,09 Univ. Trento

WV2 22 Aug 2010 PAN

MS8

0.51

2.0 17,64 17,64 FBK

WV2 22 Aug 2010 PAN

MS8

0.51

2.0 17,64 17,64 FBK

GE1 28 Sep 2011 PAN MS4

0.50 2.0

10,00 10,00 FBK

GE1 28 Sep 2011 PAN

MS4

0.50

2.0 10,00 10,00 FBK

3. PROCESSING OF VHR SATELLITE IMAGES

The WV2 image pair was acquired 22 August 2010 at circa 10:40 am (GMT). The first image was recorded in forward

scanning mode with an average in-track viewing angle of 15.9°, while the second one was acquired in reverse scanning mode

with an average in-track viewing angle of -14.0°. Cloud cover

in both images is 10% or less. The forward-looking image was delivered in 4 tiles, while the backward-looking image was

delivered in 5 tiles. A scale and radiometric example of changes between the two images is given in Fig. 2 (top). The GE1 stereo pair was acquired 28 September 2011 at circa

10:20 am (GMT). Both images were recorded in reverse

International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B1, 2012 XXII ISPRS Congress, 25 August – 01 September 2012, Melbourne, Australia

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scanning position, with a nominal in-track viewing angle of

about 15° in forward direction and -20° in backward direction

(Fig. 2, bottom). Cloud cover in both images is 4% or less. Some small errors occurred in the images (saturation, spilling),

due to the presence of reflective surfaces, in combination with the incidence angles. Fig. 3 and Fig. 4 show some examples.

Figure 2. Zoom in the stereo satellite images on the same

building block. [Top] WV2 forward-looking (left) and

backward-viewing (right) images. [Bottom] GE1 forward (left) and backward (right) images.

Figure 3. Examples of artefacts found in GE1 images.

Figure 4. Examples of artefacts in WV2 images.

3.1 Orientation and DSM generation

For the geometric processing of the WorldView-2 and GeoEye-

1 stereo-scenes, the commercial software SAT-PP (SATellite image Precision Processing) by 4DiXplorer AG (http://www.4dixplorer.com) was used. Information about the

software functionalities and the approaches for image orientation and DSM generation is given in Poli et al. (2009).

The images were oriented based on the RPC-based model, by estimating the parameters modelling an affine transformation to remove systematic errors in the given RPCs. The estimation is

run simultaneously for the two stereo images of each pair in a block adjustment. For this operation, a selection of available

ground points visible in both images was used. A sub-pixel accuracy was reached in the orientation both for WV2 and GE1

stereo-pairs.

The DSMs were generated with a multi-image least-square matching, as described in Poli et al. (2009), using a grid space

equal to 2 times the GSD, which leads to 1 m geometric resolution surface models. Few seed points were manually measured in the stereo images in correspondence of height

discontinuities to approximate the surface. The DSMs were neither manually edited nor filtered after their generation. Fig. 5

shows the DSM obtained from GE1in its full extent and two zooms in the city centre and in hilly rural area. For 3D realistic visualization, the GE1 panchromatic and

multispectral channels of the forward image were pansharpened and orthorectified on the GE1 DSM. The result is shown in Fig.

6.

Figure 5. DSM from the GE1 stereo-pair. [Top] visualization in

colour-shaded mode in SAT-PP software. [Bottom] zoom over

Trento (left) and a steep rural area (right).

International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B1, 2012 XXII ISPRS Congress, 25 August – 01 September 2012, Melbourne, Australia

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Figure 6. 3D visualization in ERDAS VirtualGIS of the textured model of Trento produced using GE1 stereo images.

3.2 DSM quality analysis

In general, the DSMs were successfully generated from WV2

and GE1 stereo images. In the mountain area on the west-south side of Trento, characterised by steep mountains and large

height difference, the shape of valleys, mountain sides and ridges and even roads is well modelled. In urban areas, building agglomerations, blocks with different heights, the road network,

some infrastructures (i.e. bridges), and rivers are well outlined.

In rural areas, adjacent fields, vegetation, and buildings are

recognised on flat or hilly terrain (Fig. 5). For quality evaluation, we compared the WV2 and GE1 DSMs with the LiDAR one in three areas, and computed the statistics

of the height differences, in terms of minimum and maximum values, mean value, standard deviation and root mean square

error (RMSE). Table 2 shows the test area location, the reference LiDAR DSM, the GE1 and WV2 DSMs and the error

maps, together with the frequency histograms and statistics.

In the error maps the height differences in the range [-1 m, 1 m] were plotted in white, as they are within the intrinsic precision

of the sensors, while large positive and negative errors were highlighted in red (LiDAR above the DSM) and blue (DSM

above LiDAR), respectively. From the analysis of the DSMs behaviour in the historic centre of Trento, characterised by small adjacent units and narrow streets, the height of the roofs is

estimated quite well. Errors are encountered between buildings,

as narrow streets are not visible in the stereo-pairs due to

shadows or occlusions. In these cases the two DSMs are above the LiDAR one, as they do not model the street level. The two large red spots (highlighted in red and blue in the LiDAR DSM)

occur on churches, both in GE1 and WV2 DSMs. The matching failure is likely due to the homogeneous material used for the

roof cover, the shadowing, and, eventually, the structure geometry. The manual measurements of seed points on the two

buildings would certainly help the matching procedure. The values in the statistics confirm the analysis. The height profiles indicates that both DSMs follow well the LiDAR profile both

on buildings and in open areas (i.e. square), being the GE1 DSM slightly more accurate than WV2 one. The matching error

in correspondence of the church roof cover is evident in the profile, too. In the train station test area, again, there is a general agreement between the two DSMs and the LiDAR one. Some

differences are due to the presence of trees (blue circle, LiDAR is below the DSMs) and to a change in the area (red circle,

LiDAR is above the DSMs), that is, a building was demolished between LiDAR and WV2/GE1 acquisitions. Regarding the

third test area (Trento Fersina), significant height differences occur in correspondence of trees (blue areas) and between tall buildings. The height profiles in one problematic area confirm

that the tall buildings are identified in the DSMs as height

peaks, but they are not completed separated, as the area between

them is occluded in the images or in shadow (Fig. 7). The error frequency histograms of GE1 and WV2 DSM follow a normal

distribution, with small lateral peaks due to the mentioned errors. The quality of GE1 DSM seems slightly better than the WV2 one, as its histograms have smaller width and higher

central peaks.

Figure 7. Example of occlusion between tall buildings in GE1

stereo-pair: forward view [left] and backward view [right].

4. CONCLUSIONS AND OUTLOOK

This paper presented the testfield set up in Trento by the 3D Optical Metrology (3DOM) Unit of Bruno Kessler Foundation (FBK) of Trento, Italy, with the aim to investigate optical

imagery, perform automatic digital surface modelling, 2D/3D feature extraction and data fusion using state-of-the-art

spaceborne, aerial and terrestrial data. With regard to spaceborne optical imagery, the testfield includes very high

resolution (VHR) stereo imagery acquired by WoldView-2 and

GeoEye-1 sensors. The images were processed with SAT-PP commercial software and two DSMs were extracted. The

quality of the DSMs was assessed using a LiDAR DSM as reference. In general, the DSMs model well the surface in flat,

hilly and mountainous areas, where cliffs, ridges and roads are well defined. In urban areas, building blocks are recognised in the historic city centre, characterised by small units closed to

each other, and individual buildings are visible in residential

and industrial areas. With respect to LiDAR, there is a general

agreement. Significant differences (larger than 1.0 m) between LiDAR and optical DSMs are encountered in case of (i) occlusions, mainly due to tall buildings or narrow streets, (ii)

homogenous texture (shadows, special roof covers), (iii) temporal changes between LiDAR and WV2/GE1 images, (iv)

temporary objects like construction sites, and (v) presence of vegetation (trees, forests), where optical sensors and LiDAR

respond differently. The statistics on three test areas shows mean values close to zero and standard deviation in the range of 6-8m due to the above mentioned problems. From a first

analysis, the performance of GE1 and WV2 sensors is similar, but deeper investigations will be conducted.

The work on the VHR spaceborne resolution imagery in the Trento testfield is planned to be further extended by carrying out more radiometric investigations, DSM generation using

other matching approaches and DSM analyses using a reference DSM from other optical sensors and excluding areas with

temporal changes. The other aerial images of the testfield Trento are currently

being processed in order to evaluate automated aerial triangulation methods, image-matching algorithms, man-made feature extraction procedures (Nex and Remondino, 2012) and

finally to estimate the PV potential on building roofs (Agugiaro et al., 2012).

International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B1, 2012 XXII ISPRS Congress, 25 August – 01 September 2012, Melbourne, Australia

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Table 2. Quality evaluation of WV2 and GE1 DSMs with respect to the LiDAR DSM: orthophoto with test areas contour (light blue)

and profile transect (yellow), LiDAR DSM, GE1 DSM, WV2 DSM, error planimetric distribution, error histograms (GE1 in blue,

WV2 in green), statistics (minimum, maximum, mean µ, standard deviation σ, RMSE) and height profiles. Measures are in metres. Trento Centre Trento Train Station Trento Fersina

Ort

ho

photo

LiD

AR

DS

M

GE

1 D

SM

Err

or

map

GE

1

min: -44.4, max: 26.5 µ: 2.3 min: -28.1, max: 53.5 µ: 1.7 min: -46.3, max: 28.8 µ: 0.5

σ: 6.6 RMSE: 6.9 σ: 6.9 RMSE: 7.1 σ: 7.4 RMSE: 7.9

WV

2 D

SM

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REFERENCES

Agugiaro, G., Nex, F., Remondino, F., Droghetti, S., De Filippi, R., Furlanello, C., 2012. Solar radiation estimation on

building roofs and web-based solar cadastre. ISPRS Annals of

Photogrammetry, Remote Sensing and Spatial Information

Sciences, XXII ISPRS Congress, Melbourne, Australia. Arefi, H., Reinartz, P., 2011. Building reconstruction from

Worldview DEM using image information. Proc. Int.

Conference on Sensors & Models in Remote Sensing &

Photogrammetry, SMPR 2011, Tehran, Iran, (on CD-ROM).

Capaldo, P., Crespi, M., Fratarcangeli, F., Nascetti, A., Pieralice, F., 2012. DSM generation from high resolution satellites imagery: applications with WorldView-1 and

GeoEye-1. Italian Journal of Remote Sensing, Vol. 44, pp. 41-53.

d'Angelo, P., Reinartz, P., 2011. Semiglobal matching results on the ISPRS stereo matching benchmark. Int. Archives of

Photogrammetry and Remote Sensing and Spatial

Information Sciences, Vol.38(4/W19), (on CD-ROM). Krauss, T., Lehner, M., Reinartz, P., 2008. Generation of coarse

3D models of urban areas from high resolution stereo satellite images. Int. Archives of Photogrammetry and Remote Sensing

and Spatial Information Sciences, Vol. 37(B1), pp. 1091-1098. ISSN 1682-1750.

Nex, F., Remondino, F., 2012. Automatic roof outlines

reconstruction from photogrammetric DSM. ISPRS Annals of

Photogrammetry, Remote Sensing and Spatial Information

Sciences, XXII ISPRS Congress, Melbourne, Australia.

Poli, D., Wolff, K., Gruen, A., 2009. Evaluation of Worldview-

1 stereo scenes and related 3D products. ISPRS Hannover

Workshop 2007, Int. Archives of the Photogrammetry,

Remote Sensing and Spatial Information Sciences, Vol. 38(1-

4-7/W5). Poli, D., Angiuli, E., Remondino, F., 2010. Radiometric and

geometric analysis of Worldview-2 stereo scenes. Int.

Archives of Photogrammetry and Remote Sensing and Spatial

Information Sciences, Vol. 38(1), Calgary, Canada, (on CD-

ROM).

Poli, D., Caravaggi, I., 2012. 3D information extraction from

stereo VHR imagery on large urban areas: lessons learned. Natural Hazards, (in press)

Poli, D., Toutin, Th., 2012. Developments in geometric

modelling for HR satellite push-broom sensors. The

Photogrammetric Record, Vol. 27(137), pp. 58-73.

ACKNOWLEDGEMENTS

This work was partly supported by the 3M project (co-founded

Marie-Curie Actions FP7 – PCOFOUND – GA-2008-226070, acronym “Trentino Project”, Bando “Incoming Team 2009”). The authors would also like to thank the Autonomous Province

of Trento (PAT) and the Municipality of Trento, for providing spatial data for the testfield, as well as Prof. Bruzzone and his

research team at RSLab (University of Trento, Italy, web: http://rslab.disi.unitn.it) for providing information about the

SPOT and the Quickbird imagery.

Err

or

map

WV

2

St

atimin: -53.9, max: 26.7 µ: 1.9 min: -39.0, max: 58.4 µ: 0.7 min: -43.7, max: 27.7 µ: 0.3

σ: 7.1 RMSE: 7.4 σ: 7.1 RMSE: 7.4 σ: 8.5 RMSE: 8.5

Err

or

his

tog

ram

s: G

E1,

WV

2

Pro

file

s: L

ida

r, G

E1, W

V2

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